{"created":"2021-03-01T06:51:11.967282+00:00","id":32519,"links":{},"metadata":{"_buckets":{"deposit":"a2514108-3300-48ad-affb-143b1db402c2"},"_deposit":{"id":"32519","owner":"1","owners":[],"pid":{"revision_id":0,"type":"depid","value":"32519"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00032519","sets":["80:4535:4597:4601","9:504:4538:4599:4602"]},"author_link":["125006","125007","125008","125009","125002","125003","125004","125005"],"item_4_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Subsurface geometry of the eastern Shonai plain active fault system, NE Japan, revealed by reprocessing industry seismic reflection data"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2006","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"2","bibliographicPageEnd":"156","bibliographicPageStart":"149","bibliographicVolumeNumber":"81","bibliographic_titles":[{"bibliographic_title":"東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo"}]}]},"item_4_description_13":{"attribute_name":"フォーマット","attribute_value_mlt":[{"subitem_description":"application/pdf","subitem_description_type":"Other"}]},"item_4_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"The eastern Shonai plain fault zone is a 40-km-long reverse fault zone bounding the western margin of the Dewa hills. Due to the lack of geophysical exploration data, the subsurface geometry of this fault system is poorly understood, especially in the southern part. Industry seismic data acquired in 1311 across the fault zone along the R. Mogami-gawa was reprocessed to reveal the subsurface geometry of the active fault system. The seismic image was improved by applying interactive velocity analysis and post-stacked migration processing. The migrated, depth-converted seismic section portrays the east-dipping faults. The eastern fault coincides with the Matusyama fault estimated by tectonic geomorphological features. The newly found fault is an east-dipping blind thrust located west of the known active fault. Based on growth strata beneath the Shonai plain, another blind fault is estimated.","subitem_description_type":"Abstract"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"125006","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Kato, Naoko"}]},{"nameIdentifiers":[{"nameIdentifier":"125007","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Sato, Hiroshi"}]},{"nameIdentifiers":[{"nameIdentifier":"125008","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Kozawa, Takshi"}]},{"nameIdentifiers":[{"nameIdentifier":"125009","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Kawanaka, Taku"}]}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/0000032519","subitem_identifier_reg_type":"JaLC"}]},"item_4_publisher_20":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"東京大学地震研究所"}]},"item_4_source_id_10":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN00162258","subitem_source_identifier_type":"NCID"}]},"item_4_source_id_8":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"00408972","subitem_source_identifier_type":"ISSN"}]},"item_4_subject_15":{"attribute_name":"日本十進分類法","attribute_value_mlt":[{"subitem_subject":"51.1","subitem_subject_scheme":"NDC"}]},"item_4_text_21":{"attribute_name":"出版者別名","attribute_value_mlt":[{"subitem_text_value":"Earthquake Research Institute, University of Tokyo"}]},"item_4_text_4":{"attribute_name":"著者所属","attribute_value_mlt":[{"subitem_text_value":"東京大学地震研究所"},{"subitem_text_value":"Earthquake Research Institute, the University of Tokyo"},{"subitem_text_value":"（株）地球科学総合研究所"},{"subitem_text_value":"JGI, Inc."}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"加藤, 直子"}],"nameIdentifiers":[{"nameIdentifier":"125002","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"佐藤, 比呂志"}],"nameIdentifiers":[{"nameIdentifier":"125003","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"小澤, 岳史"}],"nameIdentifiers":[{"nameIdentifier":"125004","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"川中, 卓"}],"nameIdentifiers":[{"nameIdentifier":"125005","nameIdentifierScheme":"WEKO"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2017-06-26"}],"displaytype":"detail","filename":"IHO81207.pdf","filesize":[{"value":"7.8MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"IHO81207.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/32519/files/IHO81207.pdf"},"version_id":"b2acef45-a8c5-441a-bd46-0c5b2b83dd95"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"active fault","subitem_subject_scheme":"Other"},{"subitem_subject":"seismic reflection profiling","subitem_subject_scheme":"Other"},{"subitem_subject":"the eastern Shonai plain fault zone","subitem_subject_scheme":"Other"},{"subitem_subject":"NE Japan","subitem_subject_scheme":"Other"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"石油探査データの再解析による庄内平野東縁断層帯の地下形状","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"石油探査データの再解析による庄内平野東縁断層帯の地下形状","subitem_title_language":"ja"}]},"item_type_id":"4","owner":"1","path":["4601","4602"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2007-04-23"},"publish_date":"2007-04-23","publish_status":"0","recid":"32519","relation_version_is_last":true,"title":["石油探査データの再解析による庄内平野東縁断層帯の地下形状"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-19T05:37:57.271377+00:00"}